mineral

Pink quartz, likely rose quartz

Quartz — silicon dioxide (SiO₂), pink variety commonly called rose quartz

AI-generated identification · may be incorrect

Pale pink, translucent to transparent, with a vitreous luster and irregular fracture; Mohs hardness 7, no cleavage, hexagonal crystal structure. The small specimen appears rough or partially tumbled, though the image is insufficient to confirm its exact mineral identity.

Identified August 20, 2026More mineral →

Explore Pink quartz, likely rose quartz in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

App Store Google Play

Physical properties

Formation & geological history

Rose quartz forms mainly in granitic pegmatites and hydrothermal veins, where trace titanium, iron, or microscopic inclusions produce the pink color. Most specimens are Precambrian to younger, depending on the host granite.

Uses & applications

Used for cabochons, beads, carvings, polished stones, and inexpensive jewelry; attractive display pieces are collected. It has limited industrial value compared with ordinary quartz.

Geological facts

Rose quartz commonly occurs massive rather than as well-formed crystals; transparent crystals are rare and may instead be pink quartz. Color can fade with prolonged strong sunlight or heat.

Field identification & locations

Identify by its pink color, glassy luster, hardness, and lack of cleavage; it should scratch glass but not be scratched by a steel knife. Common sources include Brazil, Madagascar, India, South Africa, and the United States.